Abstract

This work studies the effect of water content on the aging of APC residues, with a liquid to solid ratio ( L / S) of 0.25 or 10, aged with or without exposure to ambient air. After the residue was mixed with water, CaSO 4 and (Na,K)Al 3(SO 4) 2(OH) 6 in the raw sample yielded ettringite. When CO 2 were available, this ettringite was further transformed to gypsum, calcite and possibly gibbsite. Experimental data revealed that the concentrations of Pb, Zn, Cd, Hg, and Cu fell with age, whereas that of Cr increased. Given L / S = 10, excess Ca 2+ ions were present in the suspension, so a precipitate of primarily calcite crystals of sizes under 5 μm formed on the air–water surface. This layer significantly reduced the rates of decline of Pb, Zn, Cd and Hg contents, and also reduced the increasing rate of Cr content in the suspension. This result follows from the mass transfer barrier of CO 2 added at the air–water surface and the occurrence of subsequent chemical reactions in the suspension. An estimate of the mass transfer rate revealed that the rate-controlling step with L / S = 10 was the dissolution and diffusion of CO 2 in the bulk solution. However, at L / S = 0.25, the rate-limiting step was the dissolution of metals from ash particles. Water content is a very important process factor, whose distribution in the sample, and the resulting competition between carbonate ion flux and heavy metal flux, govern the reaction time required during the natural aging process.

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